The Global Water Cycle. OCN 401 November 12, 2015

Transcription

1 The Global Water Cycle OCN 401 November 12, 2015

2 Lecture Outline 1. The Global Water Cycle - Processes - Reservoirs and Fluxes - Composition 2. Models of the Hydrologic Cycle 3. The History of the Water Cycle - Where did planetary water come from? - What happened to the degassed water? - What has been the geologic history of sea level? 4. The Water Cycle under Scenarios of Future Climate - primary productivity - socioeconomics

3 The annual circulation of H 2 O is the largest movement of a chemical substance at the surface of the Earth The distribution of water at the Earth's surface % of total Oceans Ice caps and glaciers 2.05 Groundwater 0.68 Lakes 0.01 Soils Atmosphere (as vapor) Rivers Biosphere Total 100 %

4 Origin of water on Earth Water was delivered to primitive Earth by planetesimals, meteors and comets (Chap. 2) during its accretionary phase, which was largely complete by 3.8 billion years ago (Ga) Water was released from Earth s crust in volcanic eruptions (degassing), but remained in the atmosphere as long as Earth s surface temperature was >100 C Once Earth cooled below 100 C, most water condensed to form the oceans Enough water vapor and CO 2 remained in the atmosphere to keep the temperature of Earth s surface above freezing; without this Greenhouse effect the Earth might have remained frozen, like Mars. There is good evidence of liquid water on Earth at 3.8 bya, and the volume of water has not changed appreciably since then.

5 Global water cycle and reservoirs Units = km 3 and km 3 /yr 1 km 3 = 1x L

6 The Global Water Cycle: Fluxes and Residence Times Using estimates of the reservoir size and the magnitude of fluxes between reservoirs, can calculate the residence time (T r ) of water in each reservoir: - The T r (H 2 O) of the ocean with respect to the atmosphere: 1350 km 3 / km 3 /y = 3,176 y - The T r (H 2 O) of the ocean with respect to rivers: 1350 km 3 / 0.04 km 3 /y = 33,750 y - The T r (H 2 O) of soil water with respect to ppt or ET: 122 km 3 / 71km 3 /y = 1 y

7 Potential Evapotranspiration Average evaporation = 100 cm/yr -1 Average precipitation on land = 70cm/yr -1 Evaporation + transpiration returns ~ 70% to atmosphere Large global differences Evaporation 4 mm d -1 tropics <1 mmd -1 at poles Tropical rainforests precipitation > evaporation = river run-off Deserts precipitation = evaporation - no run off Most rainfall in the Amazon Basin derives from evapotranspiration within the basin Importance of ET implies long-term implications of deforestation for this region

8 Solar Energy Budget 70% of the sun s energy is absorbed at the Earth s surface, where it drives the hydrologic cycle.

9 Solar Energy Budget

10 Three-cell model of atmospheric circulation (1) Polar cells (2) Midlatitude cells (3) Hadley cells

11 Idealized vs. actual zonal pressure belts Non-uniform surface = uneven heating Unstable windflow = eddies Sun doesn t remain over the equator year-round = 23.5N-23.5S

12 Movement of H 2 O through the atmosphere determines the distribution of rainfall; global average precip ~943mm

13 Eastern continental margins tend to be wet, western margins dry why? Primary source of water vapor is evaporation from warm tropical & subtropical oceans In tropics & subtropics, winds are primarily from the east (Trades), carrying moist ocean air toward eastern margins of continents On east side of continents, heating by land or flow over elevation causes air to rise, forming clouds and precipitation Air flowing over the west side of the continents and adjoining eastern oceans has already been depleted of much of its water vapor & precipitation potential; e.g., Taiwan, Madagascar.

14 The availability of H 2 O on land is the single most important factor for plant growth. Net Primary Production (NPP) reflects rainfall

15 Evaporation of water is an important mechanism for transporting excess heat from the tropics to the poles through latent heat of evaporation Atmosphere transports ~ 50% of the excess heat from the tropics towards the poles Winds drive surface circulation of the ocean

16 Net evaporation from the surface ocean affects surface water salinity in the ocean and increases surface water density controlling thermohaline circulation of ocean

17 Surface water salinity in the Atlantic Ocean The maxima in evaporation-precipitation results in the highest surface water salinities in the mid-latitudes around 30 N and 30S

18 Composition of precipitation over the continental U.S. --oceanic sources as well as land-based ones

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21 Pathways of Precipitation once arriving at Earth s Surface

22 Interaction of Rainwater with Rocks and Soils at Earth s Surface Alters its Composition

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24 Precipitation > evaporation, = runoff, the main transporter of physical and chemical weathering to the sea Gibbs (1970) classification of global rivers by composition, linking river TDS to the dominant processes controlling addition of ions to rivers.

25 thinking about the global water cycle on a geologic time scale

26 Carbonate precipitation study Ca HCO > CaCO 3(s) + H 2 O + CO 2 Preferential evaporation for 16 O leads to glacial enrichment, and subsequent oceanic enrichment in 18 O The geologic record shows large changes in ocean volume, as evidenced by del 18 O of marine carbonates, that accompanied repeated glaciation during the Pleistocene Epoch

27 During the last peak glaciation (18,000 ybp) 42,000,000 km 3 of seawater was trapped in polar ice caps, or 3% of oceans volume, and this lowered sea level by 120 m relative to the present day

28 Continental glaciations thus represent a major disruption in the Earth s hydrologic cycle, or a loss of steady state conditions 18,000 ybp estimate total ppt was 14% lower than at present, deserts expanded, NPP and terrestrial biomass were lower, Erosion of exposed continental shelf sediments during glacials increased nutrient flux to the ocean, and possibly Fe leading to higher NPP --possibly creating a positive feedback on lowering P CO2

29 Melting of glaciers and ice shelves could raise sea levels by 60-80m

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31 Glacier melt increasing sea level, but major effect is thermal expansion

32 Satellite altimetry can also be used to estimate sea level rise

33 modeling the global water cycle to consider scenarios of future climate

34 Models of the Hydrologic Cycle Watershed models follow the fate of water received in ppt, and calculate runoff after subtraction of loss due to plant uptake. - The soil is defined as a collection of small boxes, in which annual input and output of water must be equal. - Water entering the soil in excess of its holding capacity is routed to the next lower soil layer, or to the next downslope unit via subsurface flow. Such models can be coupled to models of soil chemistry to predict the loss of elements in runoff. Continental scale models have been developed to assess the contribution of continental land areas to the global hydrologic cycle; coupled to GCMs, which are driven by climate, such models can predict global biogeochemical phenomena.

35 Models can be constructed that predict water movement on regional scales These can be coupled to global climate models

36 Most models predict a more humid world in response to global warming, with increased rates of water movement through the hydrologic cycle: enhanced evaporation, precipitation, runoff Not all land areas would be equally affected, with higher latitudes being disproportionately affected. Evidence consistent with this global warming effect on the hydrologic cycle includes: - increased water vapor in the stratosphere - increases in rainfall over mid-latitudes in N. hemisphere - decrease in precipitation over N. Africa - greater runoff from land

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38 Cyclical pattern of historical runoff reveals a dampening for world mean due to variance in continental cycles Recent increases in water vapor, precipitation, and streamflow are consistent with predicted changes due to a global warming --but some of this may be from reduced evapotranspiration due to reduced vegetation in some regions

39 Revisiting Regional Variability

40 The Global Water Cycle: Regional Variability Global averages obscure substantial regional differences in the hydrologic cycle. - Evaporation from the oceans ranges from 4 mm/d in the tropics to <1 mm/d at the poles. - Net evaporative loss at tropical latitudes accounts for the higher salinity of tropical oceans. - The relative balance of ppt and evap differs strongly between regions. Sources of water contributing to precipitation differ greatly regionally. - Most rainfall over the oceans is derived from seawater. - Most rainfall in the Amazon Basin derives from evapotranspiration within the basin, and long-range atmospheric transport; importance of ET implies long-term implications of deforestation for this region.

41 Facts and figures from the World Water Council 44,000 km 3 Quantity of water from rivers or aquifers to ocean 10,000-12,000 km 3 available for human consumption 4,000 km 3 global water withdrawals 2,000 km 3 global water consumption

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44 Total withdrawals and consumption Total withdrawal km3/year Total consumption km3/year Source: Shiklomanov, Future projections by D.Zimmer, based on the evolution of business as usual

45 Breakdown of water withdrawals and consumption by sector 100% 75% 50% Withdrawals Evaporation from reservoirs Withdrawal for industry Withdrawal for domestic use Withdrawal for agriculture 25% 0% % 75% 50% Consumption Consumption in industry Domestic consumption Consumption in agriculture 25% 0% Source: Shiklomanov, 1999, future projections by D.Zimmer

46 Water withdrawals and consumption for agriculture use 4000 withdrawals consumption 3000 km3 / year population (millions) Source: Shiklomanov, 1999, future projections by D.Zimmer

47 Water withdrawals and consumption for domestic use 700 withdrawals consumption 525 km3 / year population (millions) Source: Shiklomanov, 1999, future projections by D.Zimmer

48 Water withdrawals and consumption for industrial use 900 withdrawals consumption 675 km3 / year population (millions) Source: Shiklomanov, 1999, future projections by D.Zimmer

49 Figures Source: Shiklomanov, 1999, future projections by D.Zimmer

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51 Lecture Summary The global hydrologic cycle consists of various reservoirs of water on the Earth s surface, and fluxes between these reservoirs allow calculation of water residence time for each reservoir. The origin of water and its distribution into vapor vs. liquid occurred very early in Earth s history. Evidence for changes in sea level indicates fluctuations of ocean volume as a function of global climate. Global warming can significantly affect the global hydrologic cycle.

52 Changes in NPP